Stacked record for Equatorial Atlantic, presented as diff from avg Late Holocene (0 to 8 kyr) isotopic composition. The record has been linearly interpolated to 1000-year sample spacing. Dd13C=difference of d13C G. sacc and d13C U. sent of V19-30, Shackleton & Pisias, 1985, with the average Holocene difference equal to zero.